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Geomorphology of Proglacial Systems: Landform and Sediment Dynamics Recently Deglaciated Alpine Landscapes

Geomorphology of Proglacial Systems: Landform and Sediment Dynamics Recently Deglaciated Alpine Landscapes in Franklin, TN

Current price: $199.99
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Geomorphology of Proglacial Systems: Landform and Sediment Dynamics Recently Deglaciated Alpine Landscapes

Barnes and Noble

Geomorphology of Proglacial Systems: Landform and Sediment Dynamics Recently Deglaciated Alpine Landscapes in Franklin, TN

Current price: $199.99
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Size: Hardcover

This book discusses the recession of alpine glaciers since the end of the Little Ice Age (LIA), which has been accelerating in the past decades. It provides an overview of the research in the field, presenting definitions and information about the different proglacial areas and systems. A number of case studies are from the PROSA project group which encompasses the expertise of geomorphologists, geologists, glaciologists and geodesists. The PROSA joint project (High-resolution measurements of morphodynamics in rapidly changing PROglacial Systems of the Alps) is determined to tackle the problems of geomorphic activity on sediment export through a quantification of sediment fluxes effected by the aforementioned geomorphic processes within the forefield of the Gepatschferner glacier (Central Alps, Austria).
This book discusses the recession of alpine glaciers since the end of the Little Ice Age (LIA), which has been accelerating in the past decades. It provides an overview of the research in the field, presenting definitions and information about the different proglacial areas and systems. A number of case studies are from the PROSA project group which encompasses the expertise of geomorphologists, geologists, glaciologists and geodesists. The PROSA joint project (High-resolution measurements of morphodynamics in rapidly changing PROglacial Systems of the Alps) is determined to tackle the problems of geomorphic activity on sediment export through a quantification of sediment fluxes effected by the aforementioned geomorphic processes within the forefield of the Gepatschferner glacier (Central Alps, Austria).

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